Global, quasi-steady dynamics of the distant solar wind: 2. Deformation of the Heliospheric Current Sheet

1994 ◽  
Vol 99 (A3) ◽  
pp. 4185 ◽  
Author(s):  
V. J. Pizzo
Keyword(s):  
Solar Wind ◽  
Current Sheet ◽  
Heliospheric Current Sheet

Solar wind double ion beams and the heliospheric current sheet

1995 ◽  
Vol 100 (A5) ◽  
pp. 7881 ◽  
Author(s):  
C. M. Hammond ◽  
W. C. Feldman ◽  
J. L. Phillips ◽  
B. E. Goldstein ◽  
A. Balogh
Keyword(s):  
Solar Wind ◽  
Current Sheet ◽  
Heliospheric Current Sheet ◽  
Ion Beams

scholarly journals THE STRUCTURE OF THE SOLAR WIND IN THE HELIOSPHERE DEPENDING ON THE PHASE OF THE SOLAR CYCLE: LARGE-SCALE DYNAMICS OF THE HELIOSPHERIC CURRENT SHEET

2019 ◽  
Vol 47 (1) ◽  
pp. 85-87
Author(s):  
E.V. Maiewski ◽  
R.A. Kislov ◽  
H.V. Malova ◽  
O.V. Khabarova ◽  
V.Yu. Popov ◽  
...  
Keyword(s):  
Magnetic Field ◽  
Solar Wind ◽  
Solar Activity ◽  
Solar Cycle ◽  
Current Sheet ◽  
Heliospheric Current Sheet ◽  
High Solar Activity ◽  
The Sun ◽  
High Latitudes ◽  
The Magnetic Field

A stationary axisymmetric MHD model of the solar wind has been constructed, which allows us to study the spatial distribution of the magnetic field and plasma characteristics at radial distances from 20 to 400 radii of the Sun at almost all heliolatitudes. The model takes into account the changes in the magnetic field of the Sun during a quarter of the solar cycle, when the dominant dipole magnetic field is replaced by a quadrupole. Selfconsistent solutions for the magnetic and velocity fields, plasma concentration and current density of the solar wind depending on the phase of the solar cycle are obtained. It is shown that during the domination of the dipole magnetic component in the solar wind heliospheric current sheet (HCS) is located in the equatorial plane, which is a part of the system of radial and transverse currents, symmetrical in the northern and southern hemispheres. As the relative contribution of the quadrupole component to the total magnetic field increases, the shape of the HCS becomes conical; the angle of the cone gradually decreases, so that the current sheet moves entirely to one of the hemispheres. At the same time, at high latitudes of the opposite hemisphere, a second conical HCS arises, the angle of which increases. When the quadrupole field becomes dominant (at maximum solar activity), both HCS lie on conical surfaces inclined at an angle of 35 degrees to the equator. The model describes the transition from the fast solar wind at high latitudes to the slow solar wind at low latitudes: a relatively gentle transition in the period of low solar activity gives way to more drastic when high solar activity. The model also predicts an increase in the steepness of the profiles of the main characteristics of the solar wind with an increase in the radial distance from the Sun. Comparison of the obtained dependences with the available observational data is discussed.

Solar wind velocity distribution on the heliospheric current sheet during Carrington rotations 1787-1795

1995 ◽  
Vol 13 (8) ◽  
pp. 807-814
Author(s):  
B. Bala ◽  
S. R. Prabhakaran Nayar
Keyword(s):  
Solar Wind ◽  
Velocity Distribution ◽  
Current Sheet ◽  
Wind Velocity ◽  
Solar Wind Velocity ◽  
Neutral Line ◽  
Coronal Magnetic Field ◽  
Heliospheric Current Sheet ◽  
Source Surface ◽  
Low Speed

Abstract. The solar wind velocity distribution in the heliosphere is best represented using a v-map, where velocity contours are plotted in heliographic latitude-longitude coordinates. It has already been established that low-speed regions of the solar wind on the source surface correspond to the maximum bright regions of the K-corona and the neutral line of the coronal magnetic field. In this analysis, v-maps on the source surface for Carrington rotations (CRs) 1787–1795, during 1987, have been prepared using the interplanetary scintillation measurements at Research Institute of Atmospherics (RIA), Nagoya Univ., Japan. These v-maps were then used to study the time evolution of the low-speed (\\leq450 km s–1) belt of the solar wind and to deduce the distribution of solar wind velocity on the heliospheric current sheet. The low-speed belt of the solar wind on the source surface was found to change from one CR to the next, implying a time evolution. Instead of a slow and systematic evolution, the pattern of distribution of solar wind changed dramatically at one particular solar rotation (CR 1792) and the distributions for the succeeding rotations were similar to this pattern. The low-speed region, in most cases, was found to be close to the solar equator and almost parallel to it. However, during some solar rotations, they were found to be organised in certain longitudes, leaving regions with longitudinal width greater than 30° free of low-speed solar wind, i.e. these regions were occupied by solar wind with velocities greater than 450 km s–1. It is also noted from this study that the low-speed belt, in general, followed the neutral line of the coronal magnetic field, except in certain cases. The solar wind velocity on the heliospheric current sheet (HCS) varied in the range 300–585 km s–1 during the period of study, and the pattern of velocity distribution varied from rotation to rotation.

Solar wind helium and hydrogen structure near the heliospheric current sheet: A signal of coronal streamers at 1 AU

1981 ◽  
Vol 86 (A6) ◽  
pp. 4565-4573 ◽  
Author(s):  
G. Borrini ◽  
J. T. Gosling ◽  
S. J. Bame ◽  
W. C. Feldman ◽  
J. M. Wilcox
Keyword(s):  
Solar Wind ◽  
Current Sheet ◽  
Heliospheric Current Sheet ◽  
Coronal Streamers
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